carbon as early as 300° C along with a significant amount of mesopores. As the pyrolysis
temperature is increased, microporosity is retained, but the mesoporosity disappears. At
600° C the material is microporous with a monodisperse pore size distribution centered at 4–
5Å. Infrared, X-ray photoelectron, and nuclear magnetic resonance spectroscopies, in
combination with thermogravimetric analysis provide evidence that between 300 and 400° …